Skip links and keyboard navigation

Deposition and Sedimentation

Sediment deposition is the laying down of sediment carried by wind, flowing water, the sea or ice[1]. The timescale that the deposited sediment remains in place before being remobilised may be short, or, if the deposited material remains stationary over longer timescales, sedimentation takes place, with material accumulating over a surface over time.

Sediment plume in the Johnstone River, Ninds Creek. Photo by Gary Cranitch © Queensland Museum

Smaller sized, fine sediment
can remain in the water column where it can interrupt processes such at photosynthesis.

Material such as inorganic and organic sediment can be transported by (aeolian), water (fluvial/sea), or ice (cryergic)[3]. When the transportation capacity is no longer sufficient to mobilise this material, it may come to rest on a surface. This can be because of a change in the amount of energy available for transport and also because of a change in the material properties.

Sediment transported in suspension in a river may be deposited if the velocity of the water decreases. The critical velocities for erosion and deposition of different grain sizes have been modelled by Hjulström (1935)[2] and Sunborg (1956)[4].

Deposition in wetlands may occur when the slope decreases, the area increases, or the boundary roughness increases. Deposition may also occur where a river enters an estuary as the change in water chemistry to a more saline environment may cause the sediment to flocculate. This makes the particle size larger and heavier and less easily transported.

The length of time that the deposited material remains stationary on a surface can vary. For sediment to aggrade, or build up, on a surface there needs to be sufficient time and sediment supply.

Sediment processes

Treat coarse sediment

Deposition - British Geological Survey

The Rock Cycle


References

  1. ^ British Geological Survey, 'Deposition'. [online] Available at: https://www.bgs.ac.uk/discovering-geology/geological-processes/deposition/ [Accessed 24 October 2023].
  2. ^ Hjulström, F (1935), 'Studies of the morphological activity of rivers as illustrated by the river Fyris', Bull. Geol. Inst. Uppsala. [online], vol. XXV. Available at: https://paleoarchive.com/literature/Hjulstrom1935-MorphologicalActivityRiversRiverFyris.pdf.
  3. ^ Huddart, D & Stott, T (2019), Earth environments, Wiley-Blackwell, Hoboken, NJ.
  4. ^ Sundborg, Å (August 1956), 'The River Klarälven a Study of Fluvial Processes', Geografiska Annaler. [online], vol. 38, no. 2-3, pp. 125-316. Available at: https://www.tandfonline.com/doi/full/10.1080/20014422.1956.11880887 [Accessed 20 September 2023].

Last updated: 20 September 2023

This page should be cited as:

Department of Environment, Science and Innovation, Queensland (2023) Deposition and Sedimentation, WetlandInfo website, accessed 1 February 2024. Available at: https://wetlandinfo.des.qld.gov.au/wetlands/ecology/processes-systems/deposition-sedimentation/

Queensland Government
WetlandInfo   —   Department of Environment, Science and Innovation